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Although forest edges have been studied extensively as an important consequence of fragmentation, a unifying theory of edge influence has yet to be developed. Our objective was to take steps toward the development of such a theory by (1) synthesizing the current knowledge of patterns of forest structure and composition at anthropogenically created forest edges, (2) developing hypotheses about the magnitude and distance of edge influence that consider the ecological processes influencing these patterns, and (3) identifying needs for future research. We compiled data from 44 published studies on edge influence on forest structure and composition in boreal, temperate, and tropical forests. Abiotic and biotic gradients near created forest edges generate a set of primary responses to edge creation. Indirect effects from these primary responses and the original edge gradient perpetuate edge influence, leading to secondary responses. Further changes in vegetation affect the edge environment, resulting in ongoing edge dynamics. We suggest that the magnitude and distance of edge influence are a direct function of the contrast in structure and composition between adjacent communities on either side of the edge. Local factors such as climate, edge characteristics, stand attributes, and biotic factors affect patch contrast. Regional factors define the context within which to assess the ecological significance of edge influence (the degree to which the edge habitat differs from interior forest habitat). Our hypotheses will help predict edge influence on structure and composition in forested ecosystems, an important consideration for conservation. For future research on forest edges in fragmented landscapes, we encourage the testing of our hypotheses, the use of standardized methodology, complete descriptions of study sites, studies on other types of edges, synthesis of edge influence on different components of the ecosystem, and investigations of edges in a landscape context. Harper et al. Edge Influence in Fragmented Landscapes 769 Resumen: Aunque los bordes de bosque han sido extensivamente estudiados como una importante consecuencia de la fragmentación, aún no se ha desarrollado una teoría unificadora de la influencia del borde. Nuestros objetivos fueron acercarnos al desarrollo de tal teoría mediante (1) la síntesis del conocimiento actual de los patrones de estructura y composición del bosque en bordes de bosque creados antropogénicamente; (2) el desarrollo de hipótesis relacionadas con la magnitud y distancia de la influencia del borde considerando procesos ecológicos que influyen sobre esos patrones; y (3) la identificación de futuras necesidades de investigación. Recopilamos datos de 44 estudios publicados sobre la influencia del borde sobre la estructura y composición de bosques boreales, templados y tropicales. Los gradientes bióticos y abióticos creados cerca de los bordes de bosque generan una serie de respuestas primarias a la creación del borde. Los efectos indirectos de estas respuestas primarias y el borde ori...

A major challenge in predicting Earth's future climate state is to understand feedbacks that alter greenhouse-gas forcing. Here we synthesize field data from arctic Alaska, showing that terrestrial changes in summer albedo contribute substantially to recent high-latitude warming trends. Pronounced terrestrial summer warming in arctic Alaska correlates with a lengthening of the snow-free season that has increased atmospheric heating locally by about 3 watts per square meter per decade (similar in magnitude to the regional heating expected over multiple decades from a doubling of atmospheric CO2). The continuation of current trends in shrub and tree expansion could further amplify this atmospheric heating by two to seven times.

Forest age, which is affected by stand-replacing ecosystem disturbances (such as forest fires, harvesting, or insects), plays a distinguishing role in determining the distribution of carbon (C) pools and fluxes in different forested ecosystems. In this synthesis, net primary productivity (NPP), net ecosystem productivity (NEP), and five pools of C (living biomass, coarse woody debris, organic soil horizons, soil, and total ecosystem) are summarized by age class for tropical, temperate, and boreal forest biomes. Estimates of variability in NPP, NEP, and C pools are provided for each biome-age class combination and the sources of variability are discussed. Aggregated biome-level estimates of NPP and NEP were higher in intermediate-aged forests (e.g., 30-120 years), while older forests (e.g., 4120 years) were generally less productive. The mean NEP in the youngest forests (0-10 years) was negative (source to the atmosphere) in both boreal and temperate biomes (À0.1 and -1.9 Mg C ha À1 yr À1 , respectively). Forest age is a highly significant source of variability in NEP at the biome scale; for example, mean temperate forest NEP was À1.9, 4.5, 2.4, 1.9 and 1.7 Mg C ha À1 yr À1 across five age classes (0-10, 11-30, 31-70, 71-120, 121-200 years, respectively). In general, median NPP and NEP are strongly correlated (R 2 5 0.83) across all biomes and age classes, with the exception of the youngest temperate forests. Using the information gained from calculating the summary statistics for NPP and NEP, we calculated heterotrophic soil respiration (R h ) for each age class in each biome. The mean R h was high in the youngest temperate age class (9.7 Mg C ha À1 yr À1 ) and declined with age, implying that forest ecosystem respiration peaks when forests are young, not old. With notable exceptions, carbon pool sizes increased with age in all biomes, including soil C. Age trends in C cycling and storage are very apparent in all three biomes and it is clear that a better understanding of how forest age and disturbance history interact will greatly improve our fundamental knowledge of the terrestrial C cycle.

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